1. What’s So Special About ROCKS?
Rock Note Guide

2. ROCKS are….
A naturally occurring solid mixture of one or more minerals, or organic matter.

3. Rocks are classified by….
Texture: the grain size and the way grains fit together
Visible or no visible grains, shape, pattern, or overall look and feel
Textures are determined by the environment in which the rock is formed.
Composition: the minerals or grains found inside the rock
Whether it was formed in a volcano or alongside a river.

4. Types of Rocks
The three main kinds of rock are igneous, sedimentary and metamorphic rock.
Igneous rock: forms when magma/lava cools and hardens
Sedimentary rock: forms from organic and inorganic sediments
Metamorphic rock: forms when existing rock is subjected to great heat & pressure over a long period of time

5. Igneous Rocks Ignis” = Latin for “fire”
It is also called PORPHYRITIC meaning, it’s a rock that has distinct difference in it’s size of crystals.
Which these are formed from the cooling of either magma or lava
The most abundant type of rock

6. Forms BELOW ground…Intrusive
Magma cools under Earth’s Surface
Coarse Grained
Usually have LARGE crystal grains (due to cooling slowly over a long period of time)

7. Examples of Intrusive Igneous Rock

8. Forms ABOVE ground….Extrusive
Lava cools above Earth’s surface.
Fined grained
Usually has SMALL or NO crystals (due to cooling too quickly)

9. Examples of Extrusive Igneous Rocks

10. Sedimentary Rocks
Formed from sediments (rock fragments, mineral grains, animal & plant remains-shells, bones, leaves, stems).

11. Process to Make Sedimentary Rocks
1. Weathering/Erosion: where sediments get broken apart by natural force like wind, water, then transported to a new location.
2. Deposition: where sediments get laid down or placed in that new location, then can start accumulating in layers.
3. Compaction: where the weight from the layers of sediments forces out fluids and decreases the space between the grains
4. Cementation: where minerals dissolved in water crystallize between sediment grains, holding the grains together.

12. 3 Types of Sedimentary Rocks
Clastic (also called Detrial)—made of broken pieces of other rocks. Formed when rock fragments are squeezed together.

13. Clastic-Sedimentary Rocks
Shale: Formed from tiny particles of clay compacted together.
Sandstone: Forms from the compaction and cementation of small particles of sand.

14. Clastic-Sedimentary Rocks
Conglomerate: Formed from fragments of various sizes of rocks and pebbles. Fragments are rounded because they have been worn along riverbeds.
Breccia: Fragments are jagged with sharp edges. Formed from various size of rocks and pebbles.

15. 3 Types of Sedimentary Rocks:
Organic—remains of plants and animals are deposited in thick layers
Organic refers to substances that once were part of living things or were made by living things which contain calcite or calcium carbonate. (Can be tested by using acid)

16. Organic-Sedimentary Rocks
Coal: Remains of swamp plants buried in water or by volcanic ash.
Limestone: Formed by hard shells of once living things such as coral, clams, oysters, and snails. When they die their shells pile up and are covered by other sediments compacting and cementing them.

17. 3 Types of Sedimentary Rocks:
Chemical— minerals dissolved in lakes, seas, or underground water. Can occur when lakes evaporate.

18. Chemical-Sedimentary Rocks
Rock Salt: Made of the mineral halite.
Gypsum: Formed by evaporation in dry climates.

19. Metamorphic Rocks
Rocks that have changed due to intense temperature and pressure
“Meta” means “change” and morphosis means “form” in Greek
Igneous, sedimentary and other metamorphic rocks can change to become metamorphic rocks

20. What occurs in the Earth to change these rocks?
Pressure from overlying rock layers
High heat, but not enough to melt the rock
Rocks may be flattened or bent or atoms may be exchanged to form new minerals.

21. Where do metamorphic rocks usually form?
Where magma intrudes relatively cool rock
Near colliding plates (near mountain ranges)
Places that are covered miles thick with other rock causing pressure
When hot water intrudes rock
Where a meteorite strikes Earth (rare)
Where lightning bolts strike rocks (rare)

22. Classification of Metamorphic Rocks
Foliated—mineral grains are flattened and line up in parallel bands or layers.
Example: gneiss formed from rearrangement of minerals in granite into bands
Examples: Gneiss, Slate, Schist

23. Classification of Metamorphic Rocks
Non-Foliated—No bands are formed
Re-crystalization
Example: marble formed from limestone
Other examples: quartzite, Diamonds

24. Rocks Transformed
Limestone
Marble
Shale
Slate

25. Rocks Transformed
Sandstone
Quartzite
Gneiss
Mudstone
Schist or